gtcrustГеодинамика и тектонофизикаGeodynamics & Tectonophysics2078-502XInstitute of the Earth's crust of the Russian Academy of Sciences, Siberian Branch10.5800/GT-2018-9-1-0342gtcrust-526Research ArticleСОВРЕМЕННАЯ ГЕОДИНАМИКАRECENT GEODYNAMICSМИГРАЦИИ РЕАЛИЗОВАННОЙ СЕЙСМИЧЕСКОЙ ЭНЕРГИИ В РАЗЛИЧНЫХ ГЕОДИНАМИЧЕСКИХ УСЛОВИЯХMIGRATIONS OF RELEASED SEISMIC ENERGY IN VARIOUS GEODYNAMIC CONDITIONSНовопашинаА. В.NovopashinaA. V.

Анна Владимировна Новопашина, канд. геол.-мин. наук, н.с. 

Иркутск.

Anna V. Novopashina, Candidate of Geology and Mineralogy, Researcher.

Irkutsk.

anek_sanek@mail.ruСаньковВ. А.SankovV. A.

Владимир Анатольевич Саньков, канд. геол.-мин. наук, зав. лабораторией. 

Иркутск.

Vladimir A. Sankov, Candidate of Geology and Mineralogy, Head of Laboratory.

Irkutsk.

sankov@crust.irk.ruИнститут земной коры СО РАН.РоссияInstitute of the Earth’s Crust, Siberian Branch of RAS.Russian FederationИнститут земной коры СО РАН; Иркутский государственный университет.РоссияInstitute of the Earth’s Crust, Siberian Branch of RAS; Irkutsk State University.Russian Federation20182203201891139163Copyright © Новопашина А.В., Саньков В.А., 20182018Новопашина А.В., Саньков В.А.Novopashina A.V., Sankov V.A.Данная работа распространяется под лицензией Creative Commons Attribution 4.0.This work is licensed under a Creative Commons Attribution 4.0 License.https://www.gt-crust.ru/jour/article/view/526

На основе пространственно-временного анализа суммарной энергии землетрясений (LgEsum) выделен ряд свойств медленной миграции сейсмической активности для фрагментов сейсмических поясов (Центрально-Азиатского, Тихоокеанского и Альпийского): Байкальской рифтовой системы (БРС), разломной зоны Сан-Андреас (Калифорния), разломов Крайстчерч (Новая Зеландия), Северо- и Восточно-Анатолийского разломов (Турция), Филиппинской зоны субдукции и центрального фрагмента Срединно-Атлантического океанического хребта. Цепочки кластеров LgEsum маркируют распространение фронта максимальных напряжений в областях ослабления земной коры, зонах динамического влияния разломов и сочленения тектонических структур. Для процесса миграции свойственна периодичность, смена направления и близкие модульные значения скоростей в пределах сегмента единичного разлома или зоны разломов, что, вероятно, связано с механическими и реологическими свойствами земной коры и верхней мантии. Показано, что в местах периодической смены направления распространения фронта сейсмической активности в период, кратный колебаниям миграций, возможно связанный с воздействием внешних периодических факторов, может развиваться очаг сильного события. Основные периоды колебаний в миграционном процессе – 2–4 года и 9–13 лет – в разных соотношениях присутствуют в сейсмическом режиме различных сейсмических поясов. Отмечается прямая зависимость скорости миграции, а также скорости продвижения фронта максимальных напряжений от скорости межплитного движения в регионе.

The properties of slow seismic activity migration have been revealed by the space-time analysis of the total earthquake energy (LgEsum). Our study of seismic activity covers the fragments of  the Central Asian, Pacific and Alpine seismic belts: the Baikal rift system (BRS, Russia), the San Andreas fault zone (California, USA), the Christchurch fault (New Zealand), the North and East Anatolian faults (Turkey), the Philippine subduction zone, and the central fragment of the Mid-Atlantic oceanic ridge. The chains of LgEsum clusters mark the propagation of the maximum stresses front in the weaker crust areas, the zones of fault dynamic influence, and the regions of conjugated tectonic structures. The migration process is characterized by a periodicity, changes in direction, and similar modular values of the migration rates within a single fault segment (or a fault zone), which is probably related to the mechanical and rheological crust and upper mantle properties. The data analysis shows that a strong earthquake source may occur at a location wherein the front of seismic activity propagates with periodical changes in direction, and such a source can develop within a period that is multiple of the migration fluctuations, probably associated with the influence of external periodic factors. The main periods of migration fluctuations (2–4 years, and 9–13 years, in different ratios) are present in the seismic regimes of different seismic belts. The migration rate, as well as the propagation velocity of the maximum stresses front, directly depends on the velocity of movements between the plates in the region.

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The authors declare that there are no conflicts of interest present.